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The ocean's gravitational potential energy budget in a coupled climate model
Author(s) -
Butler E. D.,
Oliver K. I.,
Gregory J. M.,
Tailleux R.
Publication year - 2013
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2013gl057996
Subject(s) - buoyancy , adiabatic process , environmental science , advection , forcing (mathematics) , convection , ocean current , kinetic energy , potential energy , sink (geography) , climate model , atmospheric sciences , energy budget , climatology , mechanics , physics , ocean general circulation model , ocean dynamics , parametrization (atmospheric modeling) , general circulation model , geology , thermodynamics , climate change , oceanography , classical mechanics , cartography , geography , radiative transfer , quantum mechanics
This study examines, in a unified fashion, the budgets of ocean gravitational potential energy (GPE) and available gravitational potential energy (AGPE) in the control simulation of the coupled atmosphere‐ocean general circulation model HadCM3. Only AGPE can be converted into kinetic energy by adiabatic processes. Diapycnal mixing supplies GPE but not AGPE, whereas the reverse is true of the combined effect of surface buoyancy forcing and convection. Mixing and buoyancy forcing thus play complementary roles in sustaining the large‐scale circulation. However, the largest globally integrated source of GPE is resolved advection (+0.57 TW) and the largest sink is through parameterized eddy transports (−0.82 TW). The effect of these adiabatic processes on AGPE is identical to their effect on GPE, except for perturbations to both budgets due to numerical leakage exacerbated by nonlinearities in the equation of state.